| Titre de série : |
US Geological Survey Water-Supply Paper, 2326 -B |
| Titre : |
Sedimentary structures and textures of Rio Orinocom channel sands, Venezuela and Colombia |
| Type de document : |
texte imprimé |
| Auteurs : |
Kee, E. D. |
| Mention d'édition : |
US Geological survey |
| Editeur : |
US Geological Survey |
| Année de publication : |
1989 |
| ISBN/ISSN/EAN : |
CI-04250 |
| Note générale : |
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Sédimentation Hydrologie fluviale Terminologie |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... |
| Note de contenu : |
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... |
US Geological Survey Water-Supply Paper, 2326 -B. Sedimentary structures and textures of Rio Orinocom channel sands, Venezuela and Colombia [texte imprimé] / Kee, E. D. . - US Geological survey . - US Geological Survey, 1989. ISSN : CI-04250 Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... Langues : Anglais ( eng)
| Mots-clés : |
Sédimentation Hydrologie fluviale Terminologie |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... |
| Note de contenu : |
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ... |
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